Impact Of Chronic Hypoxia On Food Ingestion, Growth And Condition Of Atlantic Cod, Gadus Morhua ...

No abstracts are to be cited without prior reference to the author.The Gulf of St Lawrence is an enclosed sea located in Eastern Canada. It is characterised by the presence year-round of a layer of cold water (temperature < 0 °C and average salinity = 32.4) (Lauzier & Trites, 1958; Gilbert &a...

Full description

Bibliographic Details
Main Authors: Chabot, Denis, Dutil, Jean-Denis, Couturier, Christine
Format: Conference Object
Language:unknown
Published: ASC 2001 - V - Theme session 2024
Subjects:
Online Access:https://dx.doi.org/10.17895/ices.pub.25636275
https://ices-library.figshare.com/articles/conference_contribution/Impact_Of_Chronic_Hypoxia_On_Food_Ingestion_Growth_And_Condition_Of_Atlantic_Cod_Gadus_Morhua/25636275
Description
Summary:No abstracts are to be cited without prior reference to the author.The Gulf of St Lawrence is an enclosed sea located in Eastern Canada. It is characterised by the presence year-round of a layer of cold water (temperature < 0 °C and average salinity = 32.4) (Lauzier & Trites, 1958; Gilbert & Pettigrew, 1997). In winter, the water column is a two-layer system (Koutitonsky & Bugden, 1991). The permanent cold layer mixes with surface waters via storm events and density changes of surface waters caused by cold winter air temperatures. As a result, water is below 0°C from the surface down to circa 100 m. Starting in April, the water column becomes a three-layer system, with a cold intermediate layer (CIL), due to the increasing temperature and lowering salinity of surface waters (Koutitonsky & Bugden, 1991) (Gilbert & Pettigrew, 1997). In summer, the CIL is found from circa 50 to 100 m. Both surface waters and the CIL are rich in oxygen. Waters deeper than the CIL are warmer: temperature is ...